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    Reconstructed Mediterranean Salt Lens Trajectories 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 001:;page 158
    Author(s): Käse, Rolf H.; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: The existence of energetic anticyclonic mid-depth vortices of Mediterranean Water (meddies) questions the validity of a conventional advective?diffusive balance in the eastern Atlantic subtropical gyre. A mesoscale experiment ...
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    Numerical Modeling of Meander and Eddy Formation in the Azores Current Frontal Zone 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 004:;page 529
    Author(s): Kielmann, Jürgen; Käse, Rolf H.
    Publisher: American Meteorological Society
    Abstract: Numerical experiments with an 11-level primitive equation, finite-difference model in a periodic channel are performed to analyze the properties of unstable finite-amplitude disturbances in an idealized Azores Current. ...
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    Double Diffusion and the Distribution of the Density Ratio in the Mediterranean Waterfront Southeast of the Azores 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 001:;page 12
    Author(s): Washburn, Libe; Käse, Rolf H.
    Publisher: American Meteorological Society
    Abstract: Temperture and salinity (T?S) finestructure on vertical scales of 10 db and larger is examined in a 500 by 500 km grid located southeast of the Azores in the North Atlantic. The convergence of several water masses dominated ...
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    Stochastic Wind Forcing of Baroclinic Rossby Waves in the Presence of a Meridional Boundary 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 002:;page 184
    Author(s): Lippert, Angelika; Käse, Rolf H.
    Publisher: American Meteorological Society
    Abstract: The quasigeostrophic response of a continuously stratified ocean to a band-limited white-noise windstress curl is examined in an infinite and semi-infinite ocean. Baroclinic Rossby waves?predominantly of first mode ...
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    Causes of Changes in the Denmark Strait Overflow 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 006:;page 1678
    Author(s): Köhl, Armin; Käse, Rolf H.; Stammer, Detlef; Serra, Nuno
    Publisher: American Meteorological Society
    Abstract: The warming Nordic seas potentially tend to decrease the overflow across the Greenland?Iceland?Scotland Ridge (GISR) system. Recent observations by Macrander et al. document a significant drop in the intensity of outflowing ...
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    Cyclogenesis in the Denmark Strait Overflow Plume 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 011:;page 3214
    Author(s): Jungclaus, Johann H.; Hauser, Janko; Käse, Rolf H.
    Publisher: American Meteorological Society
    Abstract: A densely spaced hydrographic survey of the northern Irminger Basin together with satellite-tracked near-surface drifters confirm the intense mesoscale variability within and above the Denmark Strait overflow. In particular, ...
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    The Sensitivity of the Greenland–Scotland Ridge Overflow to Forcing Changes 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 011:;page 2307
    Author(s): Biastoch, Arne; Käse, Rolf H.; Stammer, Detlef B.
    Publisher: American Meteorological Society
    Abstract: Processes that influence the volume and heat transport across the Greenland?Scotland Ridge system are investigated in a numerical model with ?° horizontal resolution. The focus is on the sensitivity of cross-ridge transports ...
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